(Section 3.2.3.1.12)
Table 22. Differentiation characteristics of the 46° halo and the supralateral arc
Common properties These features normally are appropriate to identify the halo in the 46° region; if the halo still cannot be determined exactly by these properties, then also check the criteria for the corresponding Sun elevation
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- Halo is poorly coloured (in most cases, just red, orange and white are visible)
- No tangent arcs to the 22° halo visible, or they are significantly fainter than the 22° halo
- No infralateral arc visible
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- Halo is colourful (blue and green are also visible)
- Tangent arcs are visible, but no 22° halo, or 22° halo is very much fainter than the tangent arcs
- Supralateral arc always touches the circumzenithal arc (keep in mind that at Sun elevations between 15° and 27° also the 46° halo touches the circumzenithal arc)
- Infralateral arc is visible
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- 22° halo and tangent arcs are of similar brightness or both are well recognizable
- Halo in the 46° region has two sections that are significantly different: colourful and colourless or brighter and fainter parts
- Good displays show up both haloes simultaneously
- Infralateral arc may be visible
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Sun elevation less than 15° Supralateral arc touches 46° halo at its sides; if the Sun is near the horizon, contact arcs are at the same elevation as the Sun
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- Gap between 46° halo and circumzenithal arc
- Only the upper part of the halo is visible
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- Halo is visible at both sides only, but symmetrically
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- Very colourful or bright section at both sides of the 46° halo
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Sun elevation between 15° and 27° Identification of both halo results difficult as both haloes overlap
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- Touches circumzenithal arc
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- Touches circumzenithal arc
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- Haloes are very similar to each other; use also Common properties
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Sun elevation between 27° and 32° Haloes do not touch themselves
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- Gap between 46° halo and circumzenithal arc
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- Distance from Sun is more than 46°
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- Bright and colourful section of a halo above 46° halo
- Two separate haloes can be distinguished well
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Sun elevation more than 32° Supralateral arc does not exist at Sun elevations of more than 32°
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- Halo in 46° region is always a 46° halo
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